Category: Speakers

2024-03-23 Brian Sherrod — New Findings on Earthquakes of Salish Lowland with Tree Analysis

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We enjoyed hearing in-person USGS geologist, Dr. Brian Sherrod, on February 24, 2024 and by Zoom March 23.

THE LECTURE:  High-resolution dating of a multi-fault earthquake and earthquake recurrence in the Salish Lowland

See Sept. 2023 Science Advances article: https://www.science.org/doi/10.1126/sciadv.adh4973

Dr. Brian Sherrod discusses new evidence for a multi-fault rupture. This rupture occurred along the Seattle (SFZ) and Saddle Mountain (SM) faults in the winter of 923-924 CE. He presents new evidence for a proto-historic earthquake on the Seattle fault (in the 1830s), and he talks about recurrence of large earthquakes in the Salish Lowland. He employs photographs, USGS mapping, lidar measurements, charts, and graphs to elaborate his points. Brian is a master story-teller, and his lecture will explain how this important event was detected.

For a complete version of the research paper:  Black, Pearl, et al., 2023, A mulitfault earthquake threat for the Seattle metropolitan region revealed by mass tree mortality:  Science Advances 9, Sept. 2023

THE SPEAKER:

Dr. Brian Sherrod is a Research Geologist and Pacific Northwest Regional Coordinator for the USGS Earthquake Hazards Program, based in the Department of Earth and Space Sciences at the University of Washington.

He received his BS in Geology from James Madison University in Virginia, his MS in Geology from the University of Pittsburg, Pennsylvania, and his PhD in Geological Sciences from the University of Washington. His main area of research is paleo-seismology:  finding evidence of past earthquakes in the Pacific Northwest using geological records. Much of his work uses lidar. His recent projects include looking for evidence of surface rupture along faults in central and western Washington, coastal uplift, and subsidence along faults in the northern Salish Lowland.

 

 

2024-04-20 Ralph Haugerud – Glacial Landscape of Puget Sound

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The Lecture: Post-mortem of the southern Cordilleran Ice Sheet

Death of an ice sheet can have many causes, as shown by retreat of the southern Cordilleran Ice Sheet about 15,000 years ago. East of the Cascades, the margin of active south-flowing ice retreated north as less snow fell and more melted. West of the Cascades, the Juan de Fuca lobe of the ice sheet appears to have floated away in response to rising sea level, perhaps without a proximal climatic cause. Collapse of the Juan de Fuca lobe diverted ice from the Puget lobe, which consequently stagnated at its margin and rapidly melted back. Later Sumas ice readvance in the Fraser Lowland may reflect stabilization of the remnant ice sheet by grounding as local sea level fell, followed by climate-driven retreat.

For a more detailed abstract, please see Ralph Haugerud’s detailed abstract Jan2024.

The Speaker 

Ralph Haugerud is an exceptional geologist. Many describe him as a structural geologist and geologic mapper interested in the evolution of the Pacific Northwest, and many know about his popularity from being featured on Nick Zentner’s programs.

Ralph is a Seattle native, with BS and MS degrees from Western Washington University and a PhD from the University of Washington. He began his career looking deep in the Earth’s crust at gneiss and tonalite in the North Cascades, moved on to study turbidites, then glacial till, and now spends much of his time looking at lidar topography. He is employed by the USGS and lives in Wenatchee, Washington.

2023-11-11 Washington’s fossils—Nesbitt and Williams

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SATURDAY NOVEMBER 11, 2023

Co-authors Elizabeth Nesbitt and David B. Williams discussed their new book, Spirit Whales and Sloth Tales:  Fossils of Washington State. They provided background on what inspired them to write their book on fossils in Washington state, why they chose the fossils they did, and some of the new science that has allowed paleontologists to tease out the 500-million-year long story of life in this region. They connected the geology with fossils and illustrated how/why we have certain fossils, such as those brought in on accreted terranes and where our oldest fossils are located.

On Sunday, November 12th they presented a complementary version of this talk for the Port Townsend Marine Science Center at the Fort Worden Chapel. It  focused on the marine organisms, such as the whales, and faunas of methane seeps.

David B. Williams is an author, naturalist, and tour guide whose award-winning book, Homewaters:  A Human and Natural History of Puget Sound is a deep exploration of the stories of this beautiful waterway. He is also the author of Too High and Too Steep: Reshaping Seattle’s Topography, Stories in Stone: Travels Through Urban Geology, as well as Seattle Walks: Discovering History and Nature in the City. Williams is a Curatorial Associate at the Burke Museum and writes a free weekly newsletter, the Street Smart Naturalist (https://streetsmartnaturalist.substack.com/ – by clicking the “No thanks” you may access the previous newsletters). More information about David’s books may be found at www.geologywriter.com

Liz Nesbitt is Curator Emerita of invertebrate paleontology at the Burke Museum for Natural History and Culture, as well as, associate professor of Earth Science at the University of Washington. Her distinguished scientific contributions to the marine paleontology of the Pacific Northwest have earned many awards and honors, including having a tiny fossil snail and a fossil whale (Maiabalaena nesbittae) named for her, .

She is currently working with Burke colleagues on measuring the health of Puget Sound waters using microfauna in bottom sediments.